4.8 Article

Polarized X-ray scattering reveals non-crystalline orientational ordering in organic films

Journal

NATURE MATERIALS
Volume 11, Issue 6, Pages 536-543

Publisher

NATURE PORTFOLIO
DOI: 10.1038/NMAT3310

Keywords

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Funding

  1. DOE [DE-FG02-98ER45737, DE-AC02-05CH1123]
  2. GAANN
  3. ALS
  4. NSF [DMR 0906457, ARRA, DMR 0906224]
  5. BMBF [05 K10WEA]
  6. EPSRC [EP/E051804/1]
  7. ARC [FT100100275]
  8. LDRD under DOE [DE-AC02-05CH11231]
  9. Direct For Mathematical & Physical Scien [0906224] Funding Source: National Science Foundation
  10. Direct For Mathematical & Physical Scien
  11. Division Of Materials Research [0906457] Funding Source: National Science Foundation
  12. Division Of Materials Research [0906224] Funding Source: National Science Foundation
  13. Engineering and Physical Sciences Research Council [EP/G068356/1, EP/E051804/1] Funding Source: researchfish
  14. EPSRC [EP/E051804/1, EP/G068356/1] Funding Source: UKRI

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Molecular orientation critically influences the mechanical, chemical, optical and electronic properties of organic materials. So far, molecular-scale ordering in soft matter could be characterized with X-ray or electron microscopy techniques only if the sample exhibited sufficient crystallinity. Here, we show that the resonant scattering of polarized soft X-rays (P-SoXS) by molecular orbitals is not limited by crystallinity and that it can be used to probe molecular orientation down to size scales of 10 nm. We first apply the technique on highly crystalline small-molecule thin films and subsequently use its high sensitivity to probe the impact of liquid-crystalline ordering on charge mobility in polymeric transistors. P-SoXS also reveals scattering anisotropy in amorphous domains of all-polymer organic solar cells where interfacial interactions pattern orientational alignment in the matrix phase, which probably plays an important role in the photophysics. The energy and q-dependence of the scattering anisotropy allows the identification of the composition and the degree of orientational order in the domains.

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